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Detalle de una molasa (Prealpes suizos)

En la geología se denomina molasa a una asociación de rocas sedimentarias clásticas de origen terrestre y marino que forman depósitos costeros.[1]​ Constituyen principalmente areniscas y pizarras y se depositan en playas, lagunas, ríos y pantanos.[1]

En excavaciones superficiales admite taludes verticales de gran altura.[2]

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  • Farhan Ali Waris New Noha MOLA (a.s) say meray Nazon ka paala

Transcription

Referencias

  1. a b molasse, Encyclopedia Britannica Academic Edition. Revisado el 10 de noviembre de 2011.
  2. López M. Juan Manuel. (2006). Geología aplicada a la ingeniería civil. Madrid, Dossat 2000
Esta página se editó por última vez el 23 oct 2019 a las 11:02.
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